A long source area of the 1906 Colombia–Ecuador earthquake estimated from observed tsunami waveforms
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- Material Type
- 記事
- Title
- Author/Editor
- Yusuke YamanakaYuichiro TaniokaTakahiro Shiina
- Publication, Distribution, etc.
- Publication Date
- 2017-12-06
- Publication Date (W3CDTF)
- 2017-12-06
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 69(163)
- Volume
- 69(163)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-017-0750-z
- Persistent ID (NDL)
- info:ndljp/pid/11002689
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2017-12-14T17:18:17+09:00
- Date Captured (W3CDTF)
- 2017-12-13
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10319651
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- The 1906 Colombia-Ecuador earthquake induced both strong seismic motions and a tsunami, the most destructive earthquake in the history of the Colombia-Ecuador subduction zone. The tsunami propagated across the Pacific Ocean, and its waveforms were observed at tide gauge stations in countries including Panama, Japan, and the USA. This study conducted slip inverse analysis for the 1906 earthquake using these waveforms. A digital dataset of observed tsunami waveforms at the Naos Island (Panama) and Honolulu (USA) tide gauge stations, where the tsunami was clearly observed, was first produced by consulting documents. Next, the two waveforms were applied in an inverse analysis as the target waveform. The results of this analysis indicated that the moment magnitude of the 1906 earthquake ranged from 8.3 to 8.6. Moreover, the dominant slip occurred in the northern part of the assumed source region near the coast of Colombia, where little significant seismicity has occurred, rather than in the southern part. The results also indicated that the source area, with significant slip, covered a long distance, including the southern, central, and northern parts of the region.
- DOI
- 10.1186/s40623-017-0750-z
- Access Restrictions
- インターネット公開
- Rights (production)
- Creative Commons Attribution 4.0 International
- Related Material (URI)
- Is Referenced By
- Simulation of a Dispersive Tsunami due to the 2016 El Salvador-Nicaragua Outer-Rise Earthquake (M-w 6.9)Tsunami Resonance Characterization in Japan Due to Trans‐Pacific Sources: Response on the Bay and Continental ShelfStudy on the 1906 Colombia‐Ecuador Megathrust Earthquake Based on Tsunami Waveforms Observed at Tide Gauges: Release Variation of Accumulated Slip Deficits in the Source AreaRevising the seismic source of the 1979 Tumaco-Colombia earthquake (Mw = 8.1) for future tsunami hazard assessmentLarge amplification of the 1906 Colombia–Ecuador earthquake tsunami in Hilo Bay induced by bay-scale resonanceA numerical study on nearshore behavior of Japan Sea tsunamis using Green’s functions for Gaussian sources based on linear Boussinesq theory
- References
- Traveltime delay and initial phase reversal of distant tsunamis coupled with the self‐gravitating elastic EarthFault size and depth extent of the Ecuador earthquake (<i>M<sub>w</sub></i> 7.8) of 16 April 2016 from teleseismic and tsunami dataNew, improved version of generic mapping tools releasedGlobal Sea Floor Topography from Satellite Altimetry and Ship Depth SoundingsAn updated digital model of plate boundariesSurface deformation due to shear and tensile faults in a half-spaceThe seismic coupling of subduction zones revisitedPreliminary reference Earth modelDetermination of earthquake source parameters from waveform data for studies of global and regional seismicityThe energy release in great earthquakesThe global CMT project 2004–2010: Centroid-moment tensors for 13,017 earthquakesGlobal Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUSSecular seismic energy release in the circum-Pacific beltDepth‐dependent rupture mode along the Ecuador‐Colombia subduction zoneDistribution of discrete seismic asperities and aseismic slip along the Ecuadorian megathrustUse of the mantle magnitudeM m for the reassessment of the moment of historical earthquakesRecent crustal deformation and the earthquake cycle along the Ecuador–Colombia subduction zoneThe 16 April 2016, M7.8 (M7.5) Ecuador earthquake: A quasi-repeat of the 1942 M7.5 earthquake and partial re-rupture of the 1906 M8.6 Colombia–Ecuador earthquakeA revised tsunami source model for the 1707 Hoei earthquake and simulation of tsunami inundation of Ryujin Lake, Kyushu, JapanSlab1.0: A three‐dimensional model of global subduction zone geometriesSize of great earthquakes of 1837–1974 inferred from tsunami dataModelling of Coulomb stress changes during the great (Mw = 8.8) 1906 Colombia-Ecuador earthquakeHistorical 1942 Ecuador and 1942 Peru subduction earthquakes and earthquake cycles along Colombia-Ecuador and Peru subduction segmentsDispersion and nonlinear effects in the 2011 Tohoku‐Oki earthquake tsunamiThe rupture process of the Great 1979 Colombia Earthquake: Evidence for the asperity modelTsunami generation by horizontal displacement of ocean bottomUse of long-period surface waves for rapid determination of earthquake-source parametersRupture zones of large South American earthquakes and some predictions津波波形から推定した詳細な2003年十勝沖地震のすべり量分布Global Historical Tsunami Database
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11002689
- NAID
- 120006383816